干旱区研究 ›› 2023, Vol. 40 ›› Issue (11): 1785-1796.doi: 10.13866/j.azr.2023.11.08 cstr: 32277.14.j.azr.2023.11.08
牛子路1,2,3(),王磊1,2,3,齐拓野1,2,3(),张伊婧1,2,3,申建香1,2,3,杨竹青1,2,3,王恩田1,2,3,蒋淑汀1,2,3
收稿日期:
2023-04-07
修回日期:
2023-06-21
出版日期:
2023-11-15
发布日期:
2023-12-01
作者简介:
牛子路(1999-),男,硕士研究生,主要从事土壤盐碱化研究. E-mail: 基金资助:
NIU Zilu1,2,3(),WANG Lei1,2,3,QI Tuoye1,2,3(),ZHANG Yijing1,2,3,SHEN Jianxiang1,2,3,YANG Zhuqing1,2,3,WANG Entian1,2,3,JIANG Shuting1,2,3
Received:
2023-04-07
Revised:
2023-06-21
Published:
2023-11-15
Online:
2023-12-01
摘要:
为探究影响红寺堡扬黄灌区土壤盐渍化的主要影响因素,采用相关性分析法和主成分分析法对0~100 cm土壤剖面盐渍化特征进行研究,结果表明:(1) 研究区土壤整体为强碱性土,下层20~100 cm土壤pH值显著高于上层0~20 cm土壤pH值(P<0.05),并随着土壤深度的增加而增加,土壤全盐含量同样随土壤深度的增加而增加,呈底层高表层低的底聚型剖面特征,各层土壤全盐含量差异性不显著(P<0.05),各层土壤pH值均属于弱变异性,在空间上分布较为均匀,土壤全盐在上层0~20 cm深度属于中等变异性,在下层20~100 cm深度属于强变异性,空间分布上随着深度的变化出现差异。(2) 研究区内主要阳离子为Na++K+,各阳离子间含量差异性显著(P<0.05),阴离子主要为
牛子路, 王磊, 齐拓野, 张伊婧, 申建香, 杨竹青, 王恩田, 蒋淑汀. 宁夏红寺堡扬黄灌区土壤盐渍化特征[J]. 干旱区研究, 2023, 40(11): 1785-1796.
NIU Zilu, WANG Lei, QI Tuoye, ZHANG Yijing, SHEN Jianxiang, YANG Zhuqing, WANG Entian, JIANG Shuting. Soil salinization characteristics in irrigation region of Yellow River of Hongsipu, Ningxia[J]. Arid Zone Research, 2023, 40(11): 1785-1796.
表1
土壤全盐、pH及盐离子含量统计"
土层深度 /cm | 参数 | pH | 全盐(TS) /(mg·kg-1) | /(mg·kg-1) | /(mg·kg-1) | Cl- /(mg·kg-1) | /(mg·kg-1) | Ca2+ /(mg·kg-1) | Mg2+ /(mg·kg-1) | Na++K+ /(mg·kg-1) |
---|---|---|---|---|---|---|---|---|---|---|
0~10 (n=77) | 最小值 | 8.60 | 290.77 | 0.00 | 20.33 | 8.47 | 258.80 | 60.00 | 13.01 | 106.35 |
最大值 | 9.40 | 3218.81 | 2.77 | 164.57 | 98.67 | 1027.05 | 338.67 | 113.87 | 956.19 | |
均值 | 8.95 | 593.29 | 1.34 | 30.92 | 17.44 | 510.22 | 135.28 | 47.83 | 253.74 | |
标准差 | 0.15 | 425.45 | 0.56 | 16.79 | 11.56 | 132.48 | 37.31 | 21.68 | 143.37 | |
变异系数/% | 1.68 | 71.71 | 41.79 | 54.30 | 66.28 | 25.97 | 27.58 | 45.33 | 56.50 | |
10~20 (n=77) | 最小值 | 8.60 | 300.75 | 0.00 | 16.81 | 9.26 | 259.15 | 82.67 | 14.64 | 125.50 |
最大值 | 9.27 | 2776.36 | 3.30 | 46.50 | 71.49 | 1333.70 | 258.67 | 246.44 | 679.62 | |
均值 | 8.98 | 604.90 | 1.41 | 27.28 | 17.83 | 510.82 | 132.82 | 50.55 | 242.16 | |
标准差 | 0.15 | 425.55 | 0.66 | 6.32 | 11.15 | 173.54 | 34.49 | 33.54 | 121.70 | |
变异系数/% | 1.67 | 70.35 | 46.81 | 23.17 | 62.54 | 33.97 | 25.97 | 66.35 | 50.26 | |
20~40 (n=76) | 最小值 | 8.00 | 276.94 | 0.00 | 3.25 | 7.68 | 177.96 | 36.00 | 2.44 | 32.69 |
最大值 | 9.92 | 4699.41 | 6.00 | 95.57 | 146.53 | 1575.64 | 448.00 | 161.04 | 1197.18 | |
均值 | 9.06 | 690.53 | 1.35 | 26.75 | 19.37 | 501.03 | 128.38 | 48.79 | 238.66 | |
标准差 | 0.26 | 748.66 | 1.12 | 11.81 | 21.30 | 228.87 | 66.07 | 34.36 | 177.31 | |
变异系数/% | 2.87 | 108.42 | 82.96 | 44.15 | 109.96 | 45.68 | 51.46 | 70.42 | 74.29 | |
40~60 (n=76) | 最小值 | 8.41 | 276.71 | 0.00 | 4.47 | 5.91 | 176.89 | 56.00 | 2.44 | 33.06 |
最大值 | 9.91 | 3593.68 | 6.40 | 92.32 | 137.67 | 2363.97 | 352.00 | 407.48 | 1187.93 | |
均值 | 9.07 | 685.03 | 1.31 | 25.09 | 19.04 | 495.98 | 124.16 | 49.17 | 252.33 | |
标准差 | 0.24 | 642.03 | 1.11 | 11.64 | 19.48 | 286.14 | 65.18 | 51.32 | 184.11 | |
变异系数/% | 2.64 | 93.72 | 84.73 | 46.39 | 102.31 | 57.69 | 52.50 | 104.37 | 72.96 | |
60~80 (n=75) | 最小值 | 8.28 | 297.92 | 0.00 | 10.98 | 8.86 | 177.96 | 48.00 | 1.22 | 44.28 |
最大值 | 9.62 | 4602.75 | 4.20 | 47.58 | 150.08 | 1966.03 | 420.00 | 329.40 | 1344.53 | |
均值 | 9.08 | 818.45 | 1.30 | 24.13 | 20.53 | 502.65 | 120.29 | 55.34 | 267.85 | |
标准差 | 0.22 | 939.88 | 0.95 | 6.73 | 23.35 | 277.69 | 59.42 | 50.91 | 220.45 | |
变异系数/% | 2.42 | 114.84 | 73.08 | 27.89 | 113.74 | 55.25 | 49.40 | 91.99 | 82.30 | |
80~100 (n=74) | 最小值 | 8.16 | 323.39 | 0.00 | 4.07 | 7.68 | 205.55 | 28.00 | 2.44 | 40.41 |
最大值 | 9.91 | 5024.77 | 6.50 | 67.92 | 145.35 | 6518.8 | 1720.00 | 561.20 | 1149.78 | |
均值 | 9.08 | 825.67 | 1.23 | 24.63 | 20.00 | 587.68 | 137.92 | 61.85 | 298.33 | |
标准差 | 0.29 | 962.13 | 1.27 | 8.66 | 19.06 | 742.10 | 193.85 | 74.31 | 221.90 | |
变异系数/% | 3.19 | 116.53 | 103.25 | 35.16 | 95.30 | 126.28 | 140.55 | 120.15 | 74.38 |
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